The Schoharie Reservoir is a reservoir in the Catskill Mountains of New York State that was created to be one of 19 reservoirs that supplies New York City with water. It was created by impounding Schoharie Creek. Portions of it lie in the towns of Conesville and Gilboa in Schoharie County, Roxbury in Delaware County, and Prattsville in Greene County.
History
Even after the Ashokan Reservoir was created as New York City's thirteenth reservoir and the Kensico Reservoir was completed soon after to store its water, the water supply was still insufficient for the city's high population. A search for a new location led to the village of Gilboa, New York, which was purchased and its residents evacuated through condemnation.
Site preparation destroyed most of the area's trees and buildings up to the water line. The dam was built during the early 1920s out of stone bricks. Flooding was completed in 1924. The village of Gilboa was relocated to the west; traces of it can still be seen during a drought.
The resulting reservoir, the northernmost of the New York City system, is located 36 miles (58 km) southwest of Albany and roughly 110 miles (180 km) northwest of New York City. It lies at the southern end of Schoharie County, the northeastern end of Delaware County, and at the northwestern end of Greene County. It neighbors such towns as Gilboa, Prattsville, and Conesville. It is an impounded portion of the Schoharie Creek, a tributary of the Mohawk River, itself a tributary of the Hudson River.
The resulting reservoir consists of a single 6-mile (9.6-km) basin, and holds of water at full capacity, making it one of the smaller New York City reservoirs. Put into service in 1926, the Schoharie Reservoir provides nine million people with approximately 15-16 percent of their annual water supply needs. It is also the smaller of the two reservoirs which, along with the Ashokan Reservoir, in Olive, New York, make up the New York City Catskill Water System. Overflow from the Schoharie Reservoir tops the Gilboa Dam and runs back into Schoharie Creek, ultimately flowing into the Hudson River.
Water from the Schoharie Reservoir flows to New York City through the -long Shandaken Tunnel, and empties into the Esopus Creek at Shandaken. Another 11 miles (18 km) down the Esopus it empties into the Ashokan Reservoir. From there water enters the 92-mile (147 km) Catskill Aqueduct to the Kensico Reservoir, thence to New York City.
Gilboa Dam
The high concrete and stone brick Gilboa Dam in Schoharie County was completed in 1926. Over time the dam eroded to where it posed a potential threat to those living downstream. In December 2005, the New York City Department of Environmental Protection began a $24 million project to bring the dam up to New York State safety standards. Beginning in December 2006 eighty post-tensioned anchoring cables were installed through holes drilled in the dam into bedrock below, bringing it up to state standards. During this overhaul, residents nearby complained that their tap water had turned a brownish color, perhaps due to the intense drilling into the earth to anchor the dam.
Schoharie County planned and authorized the Gilboa Dam Failure Outdoor Warning System, which was installed by Mid-State Communications. New York City paid for the system consisting of twenty sirens stretching from the Town of Gilboa to the Town of Esperance, ending at the Montgomery County line.
A larger, full-scale overhaul of the Gilboa Dam began in the summer of 2011 after five years of planning. Estimated to cost $350 million, the project will add significant mass to the dam, install floodgates, and include a large tunnel bypass allowing water to be released safely from the reservoir into Schoharie Creek. A citizens advocacy group, called Dam Concerned Citizens, Inc., was formed to monitor structural vulnerabilities in order to ensure the safety of those living downstream.
